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The oxidation state of vanadium in titanomagnetite from layered basic intrusions

  • Etienne Balan EMAIL logo , Johan P.R. de Villiers , Sigrid Griet Eeckhout , Pieter Glatzel , Michael J. Toplis , Emmanuel Fritsch , Thierry Allard , Laurence Galoisy and Georges Calas
Published/Copyright: March 31, 2015
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Abstract

The redox conditions prevailing during the formation of vanadiferous titanomagnetites from three layered intrusions (Bushveld; Koillismaa; Skaergaard) have been estimated from the valence state of vanadium using synchrotron X-ray absorption near edge structure spectroscopy (XANES). Using a high energy-resolution X-ray emission spectrometer, we show that vanadium occurs mostly as V3+, with minor V4+. The most concentrated samples (up to 2.4 wt% V2O3) contain approximately 10% of vanadium as V4+. Both V3+ and V4+ occur in the octahedral site of the spinel structure. Considering the low magnetite/melt V4+ partition coefficients, this suggests that vanadium ores crystallized under specific oxidizing conditions.

Received: 2005-12-15
Accepted: 2006-2-23
Published Online: 2015-3-31
Published in Print: 2006-5-1

© 2015 by Walter de Gruyter Berlin/Boston

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